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AAPG Bulletin
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AAPG Bulletin; Year: 2025; Issue: April DOI: 10.1306/03182523084
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Figure 13. Sea-level apparent accommodation evolution at Fontaine de Vaucluse as a function of sea-level changes (Haq, 2014), environmental conditions, and anoxic events (Bodin et al., 2006; Godet et al., 2006; Mutterlose et al., 2009; Huck et al., 2011, 2013) from early Barremian to early Aptian. Accommodation markers are dated resulting from biostratigraphic constraints. Uncertainties related to this dating would range from 0.2 to 0.4 m.y. A = arid; C = cold; E = eutrophic; H = humid; MBE = mid-Barremian event; O = oligotrophic; OAE = ocean anoxic event; TAXY = Taxy event; W = warm.
Figure 13. Sea-level apparent accommodation evolution at Fontaine de Vaucluse as a function of sea-level changes (Haq, 2014), environmental conditions, and anoxic events (Bodin et al., 2006; Godet et al., 2006; Mutterlose et al., 2009; Huck et al., 2011, 2013) from early Barremian to early Aptian. Accommodation markers are dated resulting from biostratigraphic constraints. Uncertainties related to this dating would range from 0.2 to 0.4 m.y. A = arid; C = cold; E = eutrophic; H = humid; MBE = mid-Barremian event; O = oligotrophic; OAE = ocean anoxic event; TAXY = Taxy event; W = warm.